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Evolution and Development of Marine Biota in the Paleozoic As Affected by Abiotic Factors

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Abstract

Considering the development of biota in relation to changing abiotic factors shows that long intervals without sharp environmental changes, under transgression, active hydrodynamics, and a diversity of ecological niches, favor increases in the biodiversity of organisms. The reduction of biota is caused by quick changes in conditions, especially by multiple alternations of opposite trends (transgression – regression, warming – cooling, etc.). Moreover, negative effects arise from events expressly adverse for the development of organisms, such as the global development of anoxia in the oceans, powerful outflow of trap basalts and volcanism, and collisions of the Earth with cosmic bodies. The effects of various factors are identified especially vividly during biotic crises. Abiotic factors of the development of biota are predetermined by three fundamental causes – terrestrial (tectonics, volcanism), orbital, and cosmic. In many cases, these causes and factors predetermined by them operated simultaneously or were closely spaced on the geologic timeline. Since the cause-effect relation between them is definitely absent, we may assume that large-scale changes in the Earth's natural environment are caused by more general cosmic factors that are outside the limits of the solar system.
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